Abstract
Mechanisms giving rise to longitudinal vortices in quasi-parallel turbulent shear layers are considered. The flow is described using the Generalized Lagrangian-mean equations of Andrews & Mclntyre and is treated as a wave mean-flow interaction. Specifically, the wave field simultaneously acts both to distort the mean flow from its laminar form and account for turbulence fluctuations. Both spanwise-independent two-dimensional and three-dimensional wave fields are explored. In each case mechanisms exist to form longitudinal vortices; however the vortices grow exponentially fast only when excited by two-dimensional waves.
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© 1993 Springer Science+Business Media Dordrecht
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Phillips, W.R.C. (1993). The genesis of longitudinal vortices in free and bounded shear layers. In: Bonnet, J.P., Glauser, M.N. (eds) Eddy Structure Identification in Free Turbulent Shear Flows. Fluid Mechanics and Its Applications, vol 21. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-2098-2_5
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DOI: https://doi.org/10.1007/978-94-011-2098-2_5
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